The Journal of the Petrological Society of Korea (암석학회지)

The Petrological Society of Korea (한국암석학회)
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Characteristics of the Rock Cleavage in Jurassic Granite, Hapcheon

합천지역의 쥬라기 화강암에 발달된 결의 특성

  • Park, Deok-Won (Geologic Environment Division, Korea Institute of Geoscience and Mineral Resources)
  • 박덕원 (한국지질자원연구원 지구환경연구부)
  • Received : 2011.12.08
  • Accepted : 2011.12.23
  • Published : 2011.12.31
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Abstract

Jurassic granite from Hapcheon was analysed with respect to the characteristics of the rock cleavage. The phases of distribution of microcracks were well evidenced from the enlarged photomicrographs(${\times}6.7$) of the thin section. The planes of principal set of microcracks are parallel to the rift plane and those of secondary set are parallel to the grain plane. These rift and grain microcracks are mutually near-perpendicular on the hardway planes. Consequently the rock cleavage of Jurassic granite from the studied quarry can be related to the preferred orientation of microcracks. Microcrack parameters such as number, length and density show an order of rift > grain > hardway. These results indicate a relative magnitude of the rock cleavage. Meanwhile, brazilian tensile strengths were measured with respect to the six directions. The results revealed a strong correlation between mechanical property with microcrack parameters.

합천지역의 쥬라기 화강암에 대하여 결의 특성에 대한 분석을 실시하였다. 미세균열의 분포상은 박편의 확대사진(${\times}6.7$)에서 잘 확인되었다. 일차 우세 미세균열은 1번 면에 평행하고 이차 우세 미세균열은 2번 면에 평행하다. 이들 1번 결과 2번 결을 형성하는 미세균열은 3번 면상에서 상호 거의 수직을 이룬다. 결과적으로 연구대상 석산에서 채취한 쥬라기 화강암에서 발달하는 결은 미세균열의 배향성과 관련이 있다. 빈도수, 길이 및 밀도와 같은 미세균열의 매개변수들은 1번결 > 2번 결 > 3번 결의 순서로 우세하게 나타난다. 이러한 결과는 결의 상대적인 강도를 지시한다. 한편 6개 방향에 따른 압열 인장강도가 측정되었다. 암석의 강도와 상기한 미세균열 매개변수들 사이에는 밀접한 상관성을 보이고 있다.

Keywords

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